朝鲜半岛西北部古元古代高温变质-深熔作用:宏观和微观岩石学以及锆石U-Pb年代学制约

朝鲜半岛左接中国大陆右连日本岛链,其地质位置重要不言而喻,对其区域地质演化历史和构造属性的准确厘定,直接关系到对整个东北亚地质的全面理解和认识。本文对朝鲜半岛狼林地块西部的南浦群和甄山群的相关岩石进行了研究。野外露头、手标本和岩相学观察表明,南浦群和甄山群岩石保存了深熔作用的宏观和微观证据,矿物组合以及矿物间的反应结构表明南浦群和甄山群混合岩经历了角闪岩相到麻粒岩相的变质作用,并且在晚期熔体结晶过程中发生了逆反应或退变质过程。7件样品的锆石U-Pb定年结果显示,朝鲜半岛西北部地区在古元古代经历了多阶段(期)的变质和深熔作用过程。南浦群岩石在1917Ma可能经历了第一阶段(期)变质作用,在1877~1855Ma经历了第二阶段(期)变质深熔和石榴石持续生长,熔体冷却结晶时代为1842Ma。甄山群样品给出的变质深熔和石榴石生长的时代为1841~1830Ma,1785Ma可能代表深熔作用中抽取的熔体冷却的时代。但是,为何南浦群和甄山群样品记录的变质和深熔作用时代显示较大的差异,尚需更进一步的研究。综述前人研究成果可知,狼林地块与华北克拉通东部辽吉活动带,在变质和深熔作用类型方面存在不同之处,然而它们所记录的古元古代高温变质-深熔时代的一致性,表明二者可能至少在古元古代之前就形成了统一的大陆。     

中朝与扬子地块结合带东部的卫星重力异常特征研究

中朝板块与扬子板块碰撞结合带过黄海向东延伸方式一直是国内外学者关注的问题.本文采用最新的地球重力场模型(GGM03C)计算了中国东部海域及朝鲜半岛的360阶卫星布格重力异常,通过异常分离、水平梯度及其垂直导数等位场资料处理和边界识别技术的应用,获得与研究区地块边界及断裂相关的各种信息.结合地质资料,对中国东部海域及朝鲜半岛进行地质构造单元划分与断裂系统分析,探讨了中朝与扬子地块结合带在海区位置与东部延伸模式.对京畿地块的深部结构及地质构造的认识是探讨中朝-扬子地块结合带在朝鲜半岛所在位置的关键.分析认为,五莲-青岛-荣城断裂和嘉山-响水断裂构成中朝-扬子地块结合带的海区段,南黄海南部断裂带与绍兴-勿南沙断裂带构成中朝-华南地块结合带;在京畿地块中部可能存在近南北向的断裂带,与临津江构造带、沃川构造带和上述两个结合带共同构成中朝、扬子与华南地块结合带;南黄海属于扬子地块,而北黄海与朝鲜半岛大部分仍属于中朝地块,其南界位于济州岛南缘断裂带附近,济州岛南缘断裂带南部海域为华南地块.     

朝鲜半岛三次历史强震

本文是在整理朝鲜半岛地震史料的基础上,着重对其发生的１５４６年１３／２级地震,１６８１年７级地震、１８１０年２９／４级地震等做了详细介绍,并尝试的给出等震线图。     

大别-苏鲁造山带在朝鲜半岛的延伸方式——基于~(40)Ar/~(39)Ar构造年代学的约束

本文结合野外构造变形特征观测,在朝鲜半岛的不同构造单元采集14件糜棱岩和片麻岩样品进行~(40)Ar/~(39)Ar年代学分析,在此基础上通过对比朝鲜半岛与大别造山带不同构造单元的变形特征,探讨大别苏鲁构造带在朝鲜半岛的东延特征,取得如下认识:朝鲜半岛中部的主要构造带在中生代经历了碰撞阶段(~210Ma)、逆冲推覆(200~150Ma)、造山后伸展阶段(140~90Ma)三个主要的构造过程;从变形期次和变形特征看,临津江构造带与大别造山带的北淮阳构造带、苏鲁构造带北部威海地区具有可比性,沃川构造带与南大别构造带有相似之处;在朝鲜半岛,自临津江带至沃川带构成了较完整的中生代碰撞造山带,即大别-苏鲁造山带的东延部分,原认为的"京畿地块"应属造山带的一部分。     

汉服:漂洋过海 异域生花

中国自古有"衣冠上国、礼仪之邦"的美誉。始于黄帝,备于尧舜的汉服是华夏文明的产物,经历过辉煌也曾在"剃发易服"政策下几近消亡。我们无法忘怀在四书五     

The climate variabilities of air temperature around the Korean Peninsula

In this study, changes in climatological conditions around the Korean Peninsula are estimated quantitatively using various types of high order statistical analyses. The temperature data collected from Incheon station have been analyzed for the assessment of the climate variation. According to our analysis, the climate changes observed over the Korean Peninsula for the last century are similar to the global observational data in many respects. First of all, the warming trend [ 1.5℃ (100 yr)^-1] and the overall evolving pattern throughout the century are quite similar to each other. The temperature change in the Korean Peninsula is about two to three times larger than that of the global scale which may partially be ascribed to the influence of urbanization at mid and high latitudes. In this work, a new Winter Monsoon Index (WMI) is suggested based on the European continental scale circulation index (EU1) pattern. Our WMI is defined as the normalized sea level pressure (SLP) difference in the winter period between the centers of the East Sea and west of Lake Baikal in Siberia, the two eastern centers of the EU1 action patterns. A strong similarity is found between the time series of the WMI and surface air temperature at Incheon. The WMI has decreased gradually since the 1920s but has shifted to a rapid increasing trend in the last two decades; it was in fact accompanied by a weakening of the Siberian High and a decreasing of the northerly during winter. Our findings of the close correlations between the surface air temperature at Incheon and the WMI strongly indicate that our newly suggested index is unique and can be used as an efficient tool to predict climate variability in Korea.     

A Comparison of GPS- and NWP-derived PW Data over the Korean Peninsula

Precipitable Water (PW) derived from Global Positioning System (GPS) measurements and numerical weather prediction (NWP) model analysis data were compared to further evaluate the efficacy of applying GPS-derived PW to the NWP model. The spatial and temporal variations of GPS-derived PW during a rainfall event were also examined. GPS-derived PW measurements show good agreement with the behavior of water vapor at a high spatial resolution during the analysis period. Temporal anomalies of GPS-derived PW moving along with the front are successfully detected by the GPS array. Large positive anomalies of GPS-derived PW are indicated immediately before a rainfall event, and the intensity of these positive anomalies do not seem to decrease significantly as the precipitation system passes. These results indicate that the Korean GPS network may have great potential as a PW sensor over the Korean Peninsula. In contrast with GPS-derived PW, NWP-derived PW shows negative biases. These biases appear to stem mainly from the differences between modeled and actual GPS site elevations, as GPS sites were generally located at elevations lower than those employed by the NWP model. However, there still exists a discernable dry bias after a PW correction is applied to NWP-derived PW. GPS-derived PW better reflects the spatial and temporal moisture variations of precipitation systems, as compared to NWP-derived PW. These results provide entirely new information for improving the regional NWP system, since GPS-derived PW produced with data from the Korean GPS network may be incorporated into the NWP model to improve rainfall forecasts.     

朝鲜半岛地缘政治经济格局演变及俄罗斯政策走向评析

俄罗斯历来重视朝鲜半岛的战略地位，半岛的稳定对其地缘政治经济战略具有重要意义。本文论述了俄罗斯不断调整的朝鲜半岛政策，对其形成背景、影响和制约因素进行了分析和探讨。     

东北亚运输合作: 中国与朝鲜半岛陆路交通联系与运输组织战略

本文从促进东北亚地区经济合作健康发展角度出发,以分析预测中国与朝鲜半岛间潜在的运输需求为基础,阐述了构建中国与朝鲜半岛陆路交通联系对完善东北亚和黄海经济区交通运输体系的战略意义;构想了组织陆路交通联系的地域模式,并简要评价了不同模式的可行性和经济效益潜力。提出了以“轴－辐”模式组织中国与朝鲜半岛的陆路交通联系是最合理的观点。     

朝鲜、韩国国名探源

众所皆知，朝鲜半岛本是一统一的国家，第二次世界大战结束后根据《波茨坦协定》，由苏美军队以“三八线”为界对朝鲜分割占领，使朝鲜半岛人为地分为两部分。1948年8月，半岛南部宣布成立大韩民国；同年9月，北半部成立朝鲜民主主义人民共和国。本文介绍我们的邻邦朝鲜、韩国这两个国名以及高丽这一名称是如何得来的。